Dissolved inorganic carbon (DIC) is a key component of
the global
carbon cycle and plays a critical role in ocean acidification and
proliferation of phototrophs. Its quantification at a high spatial
resolution is essential for understanding various biogeochemical processes.
We present an analytical method for 2D chemical imaging of DIC by
combining a conventional CO2 optode with localized electrochemical
acidification from a polyaniline (PANI)-coated stainless-steel mesh
electrode. Initially, the optode response is governed by local concentrations
of free CO2 in the sample, corresponding to the established
carbonate equilibrium at the (unmodified) sample pH. Upon applying
a mild potential-based polarization to the PANI mesh, protons are
released into the sample, shifting the carbonate equilibrium toward
CO2 conversion (>99%), which corresponds to the sample
DIC. It is herein demonstrated that the CO2 optode–PANI
tandem enables the mapping of free CO2 (before PANI activation)
and DIC (after PANI activation) in complex samples, providing high
2D spatial resolution (approx. 400 μm). The significance of
this method was proven by inspecting the carbonate chemistry of complex
environmental systems, including the freshwater plant Vallisneria spiralis and lime-amended waterlogged
soil. This work is expected to pave the way for new analytical strategies
that combine chemical imaging with electrochemical actuators, aiming
to enhance classical sensing approaches via in situ (and reagentless)
sample treatment. Such tools may provide a better understanding of
environmentally relevant pH-dependent analytes related to the carbon,
nitrogen, and sulfur cycles.